- Scots Pine
Taxobox
name = Scots Pine
status = LR/lc | status_system = IUCN2.3
status_ref = [IUCN2006|assessors=Conifer Specialist Group|year=1998|id=42418|title=Pinus sylvestris|downloaded=12 May 2006]
image_width = 240px
image_caption = Scots pine,Prerow , Germany
regnum =Plant ae
divisio =Pinophyta
classis = Pinopsida
ordo =Pinales
familia =Pinaceae
genus = "Pinus"
subgenus = "Pinus"
species = "P. sylvestris"
binomial = "Pinus sylvestris"
binomial_authority = L.
range_
range_map_width = 240px
range_map_caption = DistributionThe Scots Pine ("Pinus sylvestris" L.; familyPinaceae ) is a species ofpine native toEurope andAsia , ranging fromGreat Britain andSpain east to easternSiberia , south to theCaucasus Mountains , and as far north as Lapland. In the north of its range, it occurs from sea level to 1000 m, while in the south of its range, it is a high altitude mountain tree, growing at 1200-2600 m altitude.Farjon, A. (2005). "Pines Drawings and Descriptions of the Genus Pinus" 2nd ed. Brill ISBN 90-04-13916-8.] Gymnosperm Database: [http://www.conifers.org/pi/pin/sylvestris.htm "Pinus sylvestris"] ] Mirov, N. T. (1967). "The Genus Pinus". Ronald Press.] Trees for Life: [http://www.treesforlife.org.uk/tfl.scpine.html Species profile: Scots pine] ] The Scots Pine is also the clan badge of theMcGregor Clan , one of the most famousclans fromScotland .Botany
It is an
evergreen coniferoustree growing up to 25 m in height and 1 m trunk diameter when mature, exceptionally to 35-45 m tall and 1.7 m trunk diameter and on very productive sites (inEstonia , there are some 220 year old trees that are 46 metres tall in the forests ofJärvselja Fact|date=October 2007). Thebark is thick, scaly dark grey-brown on the lower trunk, and thin, flaky and orange on the upper trunk and branches. The habit of the mature tree is distinctive due to its long, bare and straight trunk topped by a rounded or flat-topped mass of foliage. The lifespan is normally 150–300 years, with the oldest recorded specimens (in Sweden) just over 700 years.Steven, H. M., & Carlisle, A. (1959, facsimile reprint 1996). "The Native Pinewoods of Scotland". Castlepoint Press.]The shoots are light brown, with a spirally arranged scale-like pattern. On mature trees the leaves ('needles') are a glaucous blue-green, often darker green to dark yellow-green in winter, 2.5-5 cm long and 1-2 mm broad, produced in fascicles of two with a persistent grey 5–10 mm basal sheath; on vigorous young trees the leaves can be twice as long, and occasionally occur in fascicles of three or four on the tips of strong shoots. Leaf persistence varies from two to four years in warmer climates, and up to nine years in subarctic regions. Seedlings up to one year old bear juvenile leaves; these are single (not in pairs), 2–3 cm long, flattened, with a serrated margin.
The seed cones are red at pollination, then pale brown, globose and 4-8 mm diameter in their first year, expanding to full size in their second year, pointed ovoid-conic, green, then grey-green to yellow-brown at maturity, 3-7.5 cm in length. The cone scales have a flat to pyramidal apophysis, with a small prickle on the umbo. The
seed s are blackish, 3–5 mm long with a pale brown 12–20 mm wing; they are released when the cones open in spring 22–24 months after pollination. The pollen cones are yellow, occasionally pink, 8–12 mm long;pollen release is in mid to late spring.Taxonomy
Over 100 varieties have been described in the botanical literature, but only three or four are now accepted; they differ only minimally in morphology, but with more pronounced differences in genetic analysis and
resin composition. Populations in westernmost Scotland are genetically distinct from those in the rest of Scotland and northern Europe, but not sufficiently to have been distinguished as a separate botanical variety. Trees in the far north of the range were formerly sometimes treated as var. "lapponica", but the differences are clinal and it is not genetically distinct.Pravdin, L. F. (1969). "Scots Pine. Variation, intraspecific Taxonomy and Selection". Israel Program for Scientific Translations (originally published 1964 in Russian).] [Langlet, O. (1959). A Cline or not a Cline - a Question of Scots Pine. "Silvae Genetica" 8: 13-22.] [Kinloch, B. B., Westfall, R. D., & Forrest, G. I. (1986). Caledonian Scots Pine: Origins and Genetic Structure. "New Phytologist" 104: 703-729.] [Szmidt, A. E., & Wang, X-R. (1993). Molecular systematics and genetic differentiation of "Pinus sylvestris" (L.) and "P. densiflora" (Sieb. et Zucc.). "Theoret. Appl. Genet". 86: 159-165.] [Prus-Glowacki, W., & Stephan, B. R. (1994). Genetic variation of Pinus sylvestris from Spain in Relation to Other European Populations. "Silvae Genetica" 43: 7-14.] [Goncharenko, G. G., Silin, A. E., & Padutov, V. E. (1995). Intra- and interspecific genetic differentiation in closely related pines from "Pinus" subsection "Sylvestres" (Pinaceae) in the former Soviet Union. "Pl. Syst. Evol". 194: 39-54.] [Sinclair, W. T., Morman, J. D., & Ennos, R. A. (1999). The postglacial history of Scots pine ("Pinus sylvestris" L.) in western Europe: evidence from mitochondrial DNA variation. "Molec. Ecol". 8: 83-88.]
*"Pinus sylvestris" var. "sylvestris". The bulk of the range, from Scotland and Spain to central Siberia. Described above.
*"Pinus sylvestris" var. "hamata" Steven. TheBalkans , northernTurkey and theCaucasus . Foliage more consistently glaucous all year, not becoming duller in winter; cones more frequently with a pyramidal apophysis.
*"Pinus sylvestris" var. "mongolica" Litv.Mongolia and adjoining parts of southern Siberia and northwesternChina . Foliage duller green, shoots grey-green; leaves occasionally up to 12 cm long.
*"Pinus sylvestris" var. "nevadensis" D.H.Christ. The Sierra Nevada in southernSpain and possibly other Spanish populations (not considered distinct from var. "sylvestris" by all authors). Cones often with thicker scales, but doubtfully distinguishable on morphology.Ecology and conservation
Scots Pine is the only pine native to northern Europe, forming either pure forests or alongside
Norway Spruce , Common Juniper,Silver Birch , European Rowan, Eurasian Aspen and otherhardwood species. In central and southern Europe, it occurs with numerous additional species, includingEuropean Black Pine ,Mountain Pine ,Macedonian Pine , andSwiss Pine . In the eastern part of its range, it also occurs withSiberian Pine among other trees.In
Great Britain it now occurs naturally only inScotland , but historical and archaeological records indicate that it also occurred inWales andEngland until about 300-400 years ago, becoming extinct there due to over-exploitation; it has been re-introduced in these countries. Similar historical extinction and re-introduction applies toIreland ,Denmark and theNetherlands .Carlisle, A., & Brown, A. H. F. (1968). Biological Flora of the British Isles: Pinus sylvestris L. "J. Ecol.. 56: 269-307.]Scots Pine is the national tree of Scotland, and it formed much of the
Caledonian Forest which once covered much of theScottish Highlands . Overcutting fortimber demand, fire, overgrazing bysheep anddeer , and even deliberate clearance to deter wolves have all been factors in the decline of this once great pine andbirch forest. Only comparatively small areas (17,000 ha, only just over 1% of the estimated original 1,500,000 ha) of this ancient forest remain, the main surviving remnants being atAbernethy Forest ,Glen Affric ,Rothiemurchus Forest , and the Black Wood ofRannoch . Plans are currently in progress to restore at least some areas and work has started at key sites.Cultivation and uses
Scots Pine is an important tree in
forestry . The wood is used for pulp and sawntimber products. A seedling stand can be created by planting, sowing or natural regeneration. Commercialplantation rotations vary between 50-120 years, with longer rotations in northeastern areas where growth is slower. InFinland , Scots Pine was used for makingtar in the pre-industrial age. There are still some active tar producers, but mostly the industry has ceased to exist.The
wood is pale brown to red-brown, and used for general construction work. It has a drydensity of around 470 kg/m³ (varying with growth conditions), anopen porosity of 60%, afibre saturation point of 0.25 kg/kg and a saturationmoisture content of 1.60 kg/kg.Scots Pine has also been widely planted in
New Zealand and much of the colder regions ofNorth America ; it is listed as aninvasive species in some areas there, includingOntario andWisconsin . It has been widely used in the United States for theChristmas tree trade, and was one of the most popular Christmas trees from the 1950s through the 1980s. It remains popular for that usage, though it has been eclipsed in popularity, by such species asFraser Fir ,Douglas Fir , and others. Despite its invasiveness in parts of eastern North America, Scots Pine does not often grow well there, partly due to climate and soil differences between its native habitat and that of North America, and partly due to damage by pests and diseases; the tree often grows in a twisted, haphazard manner if not tended to (as they are in the Christmas tree trade).Fire Effects Information System: [http://www.fs.fed.us/database/feis/plants/tree/pinsyl/all.html "Pinus sylvestris"] ]Names
The name derives from
Latin "pinus" via French "pin" (pine); in the past (pre-18th century) this species was more often known as "Scots Fir" or "Scotch Fir" (from Danish "fyr"), but "fir" is restricted to "Abies" and "Pseudotsuga" in modern English.Other names sometimes used include Riga Pine and Norway Pine, and Mongolian Pine for var. "mongolica". "Scotch Pine" is another variant of the common name, used mostly in
North America [Germplasm Resources Information Network: [http://www.ars-grin.gov/cgi-bin/npgs/html/taxon.pl?28552 "Pinus sylvestris"] .] .Gallery
References
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